Middle to Late Ordovician arc system in the Kyrgyz Middle Tianshan: From arc-continent collision to subsequent evolution of a Palaeozoic continental margin
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Previously unknown Ordovician arc system described in the Kyrgyz Middle Tianshan

The arc is underlain by Proterozoic basement and formed from 470 to 450 Ma.

Arc-continent collision at ca. 450 Ma was accompanied by high-grade metamorphism.

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